Abstract
A study was conducted to examine the impact of moderate thermophiles (Sulphobacillus thermosulphidooxidans, Acidithiobacillus caldus, Leptospirillum ferriphilum, Sulphobacillus spp.) on four different sulfide minerals, namely pyrite, marcasite, pyrrhotite, and arsenopyrite. The study was conducted with and without the addition of iron(II) sulfate and sulfur, and the results were analyzed in terms of the dissolution of iron, nickel, and zinc. These elements play a crucial role in the formation of acid mine drainage (AMD). During the 30-day incubation period, marcasite showed the highest iron dissolution level, with the iron concentration reaching 18.81 g/L at a pH range of 1.4 to 1.6. The dissolution rates of nickel and zinc were found to be high at 87% and 74%, respectively. The addition of external iron(II) sulfate (FeSO4⋅7H2O) and sulfur (S) did not have any effect on the dissolution of nickel and zinc. It was observed that marcasite and pyrite with high iron dissolution had a higher potential for acid mine drainage (AMD) formation. On the other hand, pyrrhotite with low iron dissolution had a lower potential for AMD formation. Despite the presence of additives, arsenopyrite had little effect on AMD production. The formation of passivation layers such as ammoniojarosite and hydronium jarosite effectively suppresses the continuous extraction of iron from pyrrhotite and arsenopyrite. Based on the surface analysis of feeds and residues of samples using X-ray diffraction (XRD), scanning electron microscopy (SEM), and energy-dispersive X-ray spectroscopy (EDS), it was concluded that the surface structures had been partially disrupted due to biochemical oxidation.
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Acknowledgements
The authors are grateful to the staff of the Mineral Processing, Mine Environment and Hydrogeology Research (MEHR), and Geochemistry Laboratory of the University of Tehran for their technical assistance.
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Ali Yadollahi: investigation, methodology, software, formal analysis, validation, data curation, writing—original draft, writing—review and editing, and visualization. Hadi Abdollahi: conceptualization, methodology, validation, supervision, project administration, funding acquisition, and writing—review and editing. Faramarz Doulati Ardejani: supervision, funding acquisition, resources, and writing—review and editing. Mirsaleh Mirmohammadi: resources and funding acquisition.
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Highlights
• Biooxidation of sulfide minerals was used to evaluate AMD production.
• Dissolution of marcasite and pyrite produces AMD.
• Moderately thermophilic microorganisms dissolve Fe, Ni, and Zn.
• Jarosite precipitation can affect the biooxidation process of pyrrhotite.
• Arsenopyrite has a low iron dissolution rate due to its toxicity to bacteria.
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Yadollahi, A., Abdollahi, H., Ardejani, F.D. et al. The Impact of Moderate Thermophiles on the Production of Acid Mine Drainage and the Dissolution of Ni and Zn from Iron-Bearing Sulfide Minerals. Water Air Soil Pollut 235, 203 (2024). https://doi.org/10.1007/s11270-024-06997-7
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DOI: https://doi.org/10.1007/s11270-024-06997-7